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Britholite-(Ce) from the metaluminous granite of SW Egypt Cover

Britholite-(Ce) from the metaluminous granite of SW Egypt

Open Access
|Apr 2023

Figures & Tables

Figure 1

Geological map of southwestern Egypt (modified from EGSMA 1981). The region is a hyperarid desert with maximum daily temperatures ranging from 16°C during December to 48°C in June and rains occurring rarely.
Geological map of southwestern Egypt (modified from EGSMA 1981). The region is a hyperarid desert with maximum daily temperatures ranging from 16°C during December to 48°C in June and rains occurring rarely.

Figure 2

Photomicrographs of samples GR1 and GR2. (A) Image of a britholite prism, taken under XPL. (B) Image of a platy tabular crystal of britholite, taken under XPL. (C-D) Images of a euhedral tabular britholite, taken under PPL and XPL, showing center zonation and a resobed border. (E-F) Images of another euheral britholite, taken under PPL and XPL, showing rims around a core. Mineral abbreviations are: Bt—biotite; Bri—britholite; Mgt—magnetite; Mc—microcline; Pl—plagioclase; Qtz—quartz; Ser—sericite; Zrn—zircon; Ttn—titanite.
Photomicrographs of samples GR1 and GR2. (A) Image of a britholite prism, taken under XPL. (B) Image of a platy tabular crystal of britholite, taken under XPL. (C-D) Images of a euhedral tabular britholite, taken under PPL and XPL, showing center zonation and a resobed border. (E-F) Images of another euheral britholite, taken under PPL and XPL, showing rims around a core. Mineral abbreviations are: Bt—biotite; Bri—britholite; Mgt—magnetite; Mc—microcline; Pl—plagioclase; Qtz—quartz; Ser—sericite; Zrn—zircon; Ttn—titanite.

Figure 3

BSE images of REE grains from samples GR1 and GR2. (A) BSE image of the britholite depicted in Fig. 2E, displaying compositional zoning. (B) BSE image of another britholite crystal. In (A) and (B) the dotted red lines partially mark the original crystal outline. (C-D) BSE images of britholite grains with different levels of brightness and, hence, different chemical composition. (E-F) BSE images of britholite partially changed to REE-rich silicate.
BSE images of REE grains from samples GR1 and GR2. (A) BSE image of the britholite depicted in Fig. 2E, displaying compositional zoning. (B) BSE image of another britholite crystal. In (A) and (B) the dotted red lines partially mark the original crystal outline. (C-D) BSE images of britholite grains with different levels of brightness and, hence, different chemical composition. (E-F) BSE images of britholite partially changed to REE-rich silicate.

Figure 4

Compositions of the analyzed britholite samples in the cationic diagrams (A) P + M2+ versus Si + REE and (B) M2+ + Th + U versus 2REE (n = number of samples; R2, coefficient of determination). The ideal apatite and britholite-(Ce) endmembers are plotted as stars. Symbols: filled rectangular, Vilalva et al. 2013; open triangular, Nash 1972; open rectangular, Orlandi et al. 1989; open circular, Mulluso et al. 2012; filled circulars, Kudrina et al. 1961; filled triangular, this work.
Compositions of the analyzed britholite samples in the cationic diagrams (A) P + M2+ versus Si + REE and (B) M2+ + Th + U versus 2REE (n = number of samples; R2, coefficient of determination). The ideal apatite and britholite-(Ce) endmembers are plotted as stars. Symbols: filled rectangular, Vilalva et al. 2013; open triangular, Nash 1972; open rectangular, Orlandi et al. 1989; open circular, Mulluso et al. 2012; filled circulars, Kudrina et al. 1961; filled triangular, this work.

Figure 5

Modal data of the samples GR1 and GR2 plotted on the IUGS quartz-alkaline feldspar-plagioclase diagram of the plutonic rocks.
Modal data of the samples GR1 and GR2 plotted on the IUGS quartz-alkaline feldspar-plagioclase diagram of the plutonic rocks.

SEM-EDS analyses (wt%) of duplicate mineral spots (A and B) from GR1 and GR2; BDL—below detecton limit_

AB± 1σ% Errors
Britholite
SiO217.1015.900.603.64
ThO7.008.340.548.73
UO2BDLBDL
ZrOBDLBDL
Al2O37.906.820.547.34
La2O313.3015.100.906.34
Ce2O324.7026.701.003.89
Pr2O32.201.940.136.28
Nd2O35.005.150.071.48
Sm2O3BDLBDL
Gd2O3BDLBDL
FeO8.007.580.212.69
Cr2O3BDLBDL
MgO4.303.120.5916.0
CaO5.906.500.304.80
Na2O1.240.650.3031.22
K2O0.530.800.1320.30
P2O5BDLBDL
SO30.270.200.0314.89
F2.511.070.7240.28
Total99.9599.87
Magnetite
SiO22.402.400.000.00
Al2O30.600.800.1014.28
FeO93.8094.700.450.48
Cr2O31.140.740.2021.28
MgO0.300.400.0514.29
Na2O0.701.000.1517.65
Total98.94100.04
Zircon
SiO229.8028.300.752.58
ZrO68.1067.800.150.22
Al2O30.300.300.000.00
FeO0.701.300.3030.00
CaO0.600.300.3033.33
Na2O0.500.900.2028.57
Total100.098.90
DOI: https://doi.org/10.2478/mipo-2023-0002 | Journal eISSN: 1899-8526 | Journal ISSN: 1899-8291
Language: English
Page range: 11 - 17
Submitted on: Dec 12, 2022
Accepted on: Feb 20, 2023
Published on: Apr 6, 2023
Published by: Mineralogical Society of Poland
In partnership with: Paradigm Publishing Services
Publication frequency: 1 issue per year

© 2023 Kamaleldin M. Hassan, published by Mineralogical Society of Poland
This work is licensed under the Creative Commons Attribution 4.0 License.